The document discusses the rock cycle and the three main types of rocks - igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling of magma, either underground to form intrusive igneous rocks or on the surface to form extrusive igneous rocks. Sedimentary rocks form through the weathering of existing rocks and the deposition of sediments. Metamorphic rocks form from heat and pressure altering existing rocks deep underground. The rock cycle describes how rocks continuously change from one type to another through geological processes.
- Rocks are naturally occurring mixtures of minerals, mineraloids, glass or organic matter that are divided into three main types - igneous, sedimentary, and metamorphic - based on how they were formed.
- Igneous rocks form from the cooling of magma or lava either below or above ground. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form from changes to existing rocks through heat, pressure, and chemical reactions in the Earth.
- Rocks are constantly changing between these three types through the rock cycle as they are weathered, eroded, melted, cooled, and subjected to pressure and heat within the Earth.
The document discusses the three main types of rocks - igneous, sedimentary, and metamorphic - and the rock cycle by which rocks are formed and changed over time. It explains that igneous rocks form from cooling magma, sedimentary rocks form through compaction or cementation of sediments, and metamorphic rocks form from extreme heat and pressure changing existing rock types. The rock cycle involves the continuous transformation of rocks between these types through geological forces and processes.
This document discusses the three main types of rocks - igneous, sedimentary, and metamorphic - and the rock cycle. It explains that igneous rocks form from cooling magma, sedimentary rocks form through compaction or cementation of sediments, and metamorphic rocks form from extreme heat and pressure changing existing rocks. The rock cycle is also summarized, noting that geological forces cause rocks to change forms over time, passing through the different types.
This document defines rocks and describes the three main types of rocks: igneous, sedimentary, and metamorphic. It explains that rocks are divided based on how they were formed and can change between types through geological processes. The rock cycle diagram shows how rocks continuously change between igneous, sedimentary and metamorphic forms over millions of years through melting, cooling, burial and erosion.
This document discusses petrology, which is the branch of geology that studies rocks and the conditions under which they form. It describes the three main classes of rocks - igneous, sedimentary, and metamorphic - and their key characteristics. Igneous rocks form from cooling magma, either deep underground as plutonic rocks or at the surface as volcanic rocks. Sedimentary rocks are formed from the lithification of sediments. Metamorphic rocks form from the alteration of existing rocks through heat, pressure, and chemically active fluids in the Earth's crust.
The document discusses the rock cycle and the three main types of rocks - igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling of magma, either underground to form intrusive igneous rocks or on the surface to form extrusive igneous rocks. Sedimentary rocks form through the weathering of existing rocks and the deposition of sediments. Metamorphic rocks form from heat and pressure altering existing rocks deep underground. The rock cycle describes how rocks continuously change from one type to another through geological processes.
- Rocks are naturally occurring mixtures of minerals, mineraloids, glass or organic matter that are divided into three main types - igneous, sedimentary, and metamorphic - based on how they were formed.
- Igneous rocks form from the cooling of magma or lava either below or above ground. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form from changes to existing rocks through heat, pressure, and chemical reactions in the Earth.
- Rocks are constantly changing between these three types through the rock cycle as they are weathered, eroded, melted, cooled, and subjected to pressure and heat within the Earth.
The document discusses the three main types of rocks - igneous, sedimentary, and metamorphic - and the rock cycle by which rocks are formed and changed over time. It explains that igneous rocks form from cooling magma, sedimentary rocks form through compaction or cementation of sediments, and metamorphic rocks form from extreme heat and pressure changing existing rock types. The rock cycle involves the continuous transformation of rocks between these types through geological forces and processes.
This document discusses the three main types of rocks - igneous, sedimentary, and metamorphic - and the rock cycle. It explains that igneous rocks form from cooling magma, sedimentary rocks form through compaction or cementation of sediments, and metamorphic rocks form from extreme heat and pressure changing existing rocks. The rock cycle is also summarized, noting that geological forces cause rocks to change forms over time, passing through the different types.
This document defines rocks and describes the three main types of rocks: igneous, sedimentary, and metamorphic. It explains that rocks are divided based on how they were formed and can change between types through geological processes. The rock cycle diagram shows how rocks continuously change between igneous, sedimentary and metamorphic forms over millions of years through melting, cooling, burial and erosion.
This document discusses petrology, which is the branch of geology that studies rocks and the conditions under which they form. It describes the three main classes of rocks - igneous, sedimentary, and metamorphic - and their key characteristics. Igneous rocks form from cooling magma, either deep underground as plutonic rocks or at the surface as volcanic rocks. Sedimentary rocks are formed from the lithification of sediments. Metamorphic rocks form from the alteration of existing rocks through heat, pressure, and chemically active fluids in the Earth's crust.
Rocks are naturally occurring mixtures of minerals, mineraloids, or organic matter that are divided into three main types - igneous, sedimentary, and metamorphic - based on their formation process. Rocks are continually changed over time through the rock cycle as they are weathered, eroded, melted, cooled, cemented, and subjected to heat and pressure, allowing them to transition between the three rock types. The composition and origins of rocks, such as whether they formed from magma, sediments, or changed forms due to heat and pressure, are used to classify the different types of rocks.
Rocks are naturally occurring aggregates composed of minerals and mineraloids. There are three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling of magma either underground (intrusive) or above ground (extrusive). Sedimentary rocks form from the lithification of sediments. Metamorphic rocks form from changes to existing rocks through heat, pressure, and chemical processes within the earth. Minerals have properties such as crystal structure, hardness, and chemical composition that are used to identify different types.
This document defines and describes the three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling of magma or lava. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form from existing rocks undergoing changes due to heat and pressure in the Earth. Rocks can change between these types through geological processes in the rock cycle.
This document defines rocks and describes the three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling of magma or lava. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form from existing rocks undergoing changes due to heat and pressure in the Earth. Rocks can change between these types through geological processes in the rock cycle.
There are three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling and solidification of magma either below or above the ground. Sedimentary rocks form from the compression of sediments and organic materials. Metamorphic rocks form from the alteration of existing igneous and sedimentary rocks through heat, pressure, and chemical changes. Rocks continuously change between these forms through the rock cycle as they are weathered, buried deep underground, and altered by melting.
Rocks are naturally occurring mixtures of minerals, glass, or organic matter that are divided into three main types based on their formation: igneous, sedimentary, and metamorphic. Igneous rocks form from cooling magma or lava. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form from existing igneous or sedimentary rocks that have been changed by heat, pressure, and chemical reactions in Earth's crust. Rocks can change between these types through geological processes in a continuous cycle.
1. Igneous rock is formed from the solidification of magma or lava emerging from depth.
2. Igneous rocks can be classified based on the temperature and pressure conditions under which they form.
3. Bowen's reaction series shows the progression of silicate mineral crystallization at specific temperatures.
Rocks are naturally occurring mixtures that can be divided into three main types - igneous, sedimentary, and metamorphic - based on their formation process. Igneous rocks form from cooling magma or lava. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form from changes to existing rocks through heat, pressure, and other processes in the Earth. Rocks continually change between these types through the rock cycle as they are weathered, eroded, melted, cooled, and compacted over time.
The document discusses the rock cycle and how different types of rocks are formed. It describes:
1) The rock cycle is a series of changes where geological forces cause rocks to change from one type to another, such as igneous to sedimentary or metamorphic.
2) Igneous rocks form from the cooling of magma, either below ground (intrusive) or above ground (extrusive). Sedimentary rocks form from the compaction or cementation of sediments.
3) Metamorphic rocks are formed from existing rocks that undergo changes from heat, pressure, and chemical processes deep underground.
This document discusses the three main types of rocks: igneous, sedimentary, and metamorphic. It describes the rock cycle which shows how the different rock types are interrelated through geological processes. Igneous rocks form from the cooling of magma, either underground to form intrusive igneous rocks or on the surface to form extrusive igneous rocks like lava. Sedimentary rocks are formed at the surface through the weathering of existing rocks, erosion, deposition of sediments, and cementation. Metamorphic rocks form from the alteration of existing rocks deep underground through heat, pressure, and chemically active fluids.
Rocks are a combination of minerals that are bonded together in some way.
All rocks are made of minerals
Monomineralic- contain one mineral
Polymineralic- contain more than one mineral
Rocks are classified into three groups by how they are formed
Igneous Rocks
Sedimentary rock
Metamorphic rock
The document outlines learning outcomes for a lesson on rock types:
a) Identify and describe the three basic rock types;
b) Describe how each rock type forms and define their environments;
c) Describe how rocks are transformed through the rock cycle;
d) Identify and describe geologic processes in the rock cycle.
The document discusses the three main rock types - igneous, sedimentary, and metamorphic rocks. It describes the rock cycle which shows how the different rock types are interrelated through geological processes. Igneous rocks form from the cooling of magma, either below ground (intrusive) or on the surface (extrusive). Sedimentary rocks form through the weathering of existing rocks, erosion, deposition of sediments, and compaction/cementation. Metamorphic rocks form from the alteration of existing rocks deep underground under high pressures and temperatures.
The document discusses the three main rock types - igneous, sedimentary, and metamorphic rocks. It describes the rock cycle which shows how the different rock types are interrelated through geological processes. Igneous rocks form from the cooling of magma, either below ground (intrusive) or on the surface (extrusive). Sedimentary rocks form through the weathering of existing rocks, erosion and deposition of sediments, and compaction and cementation over time. Metamorphic rocks form from the alteration of existing rocks deep underground under high pressures and temperatures.
The document describes the three main types of rocks - igneous, sedimentary, and metamorphic. It explains that igneous rocks form from the cooling of magma, sedimentary rocks form from the compaction of sediments, and metamorphic rocks form from the alteration of existing rocks due to heat and pressure. The rock cycle is also discussed, which illustrates how rocks continuously form, change, and erode over time. Various sub-types and characteristics of each rock type are provided as examples.
The document outlines specific learning outcomes for a lesson on rock types. At the end of the lesson, students will be able to: identify and describe the three basic rock types; describe how each rock type forms and define their environments of formation; describe how rocks are transformed through the rock cycle; and identify and describe different geologic processes in the rock cycle.
The document outlines specific learning outcomes for a lesson on rock types. At the end of the lesson, students will be able to: identify and describe the three basic rock types; describe how each rock type forms and define their environments of formation; describe how rocks are transformed through the rock cycle; and identify and describe different geologic processes in the rock cycle.
Immersive Learning That Works: Research Grounding and Paths ForwardLeonel Morgado
We will metaverse into the essence of immersive learning, into its three dimensions and conceptual models. This approach encompasses elements from teaching methodologies to social involvement, through organizational concerns and technologies. Challenging the perception of learning as knowledge transfer, we introduce a 'Uses, Practices & Strategies' model operationalized by the 'Immersive Learning Brain' and ‘Immersion Cube’ frameworks. This approach offers a comprehensive guide through the intricacies of immersive educational experiences and spotlighting research frontiers, along the immersion dimensions of system, narrative, and agency. Our discourse extends to stakeholders beyond the academic sphere, addressing the interests of technologists, instructional designers, and policymakers. We span various contexts, from formal education to organizational transformation to the new horizon of an AI-pervasive society. This keynote aims to unite the iLRN community in a collaborative journey towards a future where immersive learning research and practice coalesce, paving the way for innovative educational research and practice landscapes.
Unlocking the mysteries of reproduction: Exploring fecundity and gonadosomati...AbdullaAlAsif1
The pygmy halfbeak Dermogenys colletei, is known for its viviparous nature, this presents an intriguing case of relatively low fecundity, raising questions about potential compensatory reproductive strategies employed by this species. Our study delves into the examination of fecundity and the Gonadosomatic Index (GSI) in the Pygmy Halfbeak, D. colletei (Meisner, 2001), an intriguing viviparous fish indigenous to Sarawak, Borneo. We hypothesize that the Pygmy halfbeak, D. colletei, may exhibit unique reproductive adaptations to offset its low fecundity, thus enhancing its survival and fitness. To address this, we conducted a comprehensive study utilizing 28 mature female specimens of D. colletei, carefully measuring fecundity and GSI to shed light on the reproductive adaptations of this species. Our findings reveal that D. colletei indeed exhibits low fecundity, with a mean of 16.76 ± 2.01, and a mean GSI of 12.83 ± 1.27, providing crucial insights into the reproductive mechanisms at play in this species. These results underscore the existence of unique reproductive strategies in D. colletei, enabling its adaptation and persistence in Borneo's diverse aquatic ecosystems, and call for further ecological research to elucidate these mechanisms. This study lends to a better understanding of viviparous fish in Borneo and contributes to the broader field of aquatic ecology, enhancing our knowledge of species adaptations to unique ecological challenges.
Rocks are naturally occurring mixtures of minerals, mineraloids, or organic matter that are divided into three main types - igneous, sedimentary, and metamorphic - based on their formation process. Rocks are continually changed over time through the rock cycle as they are weathered, eroded, melted, cooled, cemented, and subjected to heat and pressure, allowing them to transition between the three rock types. The composition and origins of rocks, such as whether they formed from magma, sediments, or changed forms due to heat and pressure, are used to classify the different types of rocks.
Rocks are naturally occurring aggregates composed of minerals and mineraloids. There are three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling of magma either underground (intrusive) or above ground (extrusive). Sedimentary rocks form from the lithification of sediments. Metamorphic rocks form from changes to existing rocks through heat, pressure, and chemical processes within the earth. Minerals have properties such as crystal structure, hardness, and chemical composition that are used to identify different types.
This document defines and describes the three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling of magma or lava. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form from existing rocks undergoing changes due to heat and pressure in the Earth. Rocks can change between these types through geological processes in the rock cycle.
This document defines rocks and describes the three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling of magma or lava. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form from existing rocks undergoing changes due to heat and pressure in the Earth. Rocks can change between these types through geological processes in the rock cycle.
There are three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling and solidification of magma either below or above the ground. Sedimentary rocks form from the compression of sediments and organic materials. Metamorphic rocks form from the alteration of existing igneous and sedimentary rocks through heat, pressure, and chemical changes. Rocks continuously change between these forms through the rock cycle as they are weathered, buried deep underground, and altered by melting.
Rocks are naturally occurring mixtures of minerals, glass, or organic matter that are divided into three main types based on their formation: igneous, sedimentary, and metamorphic. Igneous rocks form from cooling magma or lava. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form from existing igneous or sedimentary rocks that have been changed by heat, pressure, and chemical reactions in Earth's crust. Rocks can change between these types through geological processes in a continuous cycle.
1. Igneous rock is formed from the solidification of magma or lava emerging from depth.
2. Igneous rocks can be classified based on the temperature and pressure conditions under which they form.
3. Bowen's reaction series shows the progression of silicate mineral crystallization at specific temperatures.
Rocks are naturally occurring mixtures that can be divided into three main types - igneous, sedimentary, and metamorphic - based on their formation process. Igneous rocks form from cooling magma or lava. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form from changes to existing rocks through heat, pressure, and other processes in the Earth. Rocks continually change between these types through the rock cycle as they are weathered, eroded, melted, cooled, and compacted over time.
The document discusses the rock cycle and how different types of rocks are formed. It describes:
1) The rock cycle is a series of changes where geological forces cause rocks to change from one type to another, such as igneous to sedimentary or metamorphic.
2) Igneous rocks form from the cooling of magma, either below ground (intrusive) or above ground (extrusive). Sedimentary rocks form from the compaction or cementation of sediments.
3) Metamorphic rocks are formed from existing rocks that undergo changes from heat, pressure, and chemical processes deep underground.
This document discusses the three main types of rocks: igneous, sedimentary, and metamorphic. It describes the rock cycle which shows how the different rock types are interrelated through geological processes. Igneous rocks form from the cooling of magma, either underground to form intrusive igneous rocks or on the surface to form extrusive igneous rocks like lava. Sedimentary rocks are formed at the surface through the weathering of existing rocks, erosion, deposition of sediments, and cementation. Metamorphic rocks form from the alteration of existing rocks deep underground through heat, pressure, and chemically active fluids.
Rocks are a combination of minerals that are bonded together in some way.
All rocks are made of minerals
Monomineralic- contain one mineral
Polymineralic- contain more than one mineral
Rocks are classified into three groups by how they are formed
Igneous Rocks
Sedimentary rock
Metamorphic rock
The document outlines learning outcomes for a lesson on rock types:
a) Identify and describe the three basic rock types;
b) Describe how each rock type forms and define their environments;
c) Describe how rocks are transformed through the rock cycle;
d) Identify and describe geologic processes in the rock cycle.
The document discusses the three main rock types - igneous, sedimentary, and metamorphic rocks. It describes the rock cycle which shows how the different rock types are interrelated through geological processes. Igneous rocks form from the cooling of magma, either below ground (intrusive) or on the surface (extrusive). Sedimentary rocks form through the weathering of existing rocks, erosion, deposition of sediments, and compaction/cementation. Metamorphic rocks form from the alteration of existing rocks deep underground under high pressures and temperatures.
The document discusses the three main rock types - igneous, sedimentary, and metamorphic rocks. It describes the rock cycle which shows how the different rock types are interrelated through geological processes. Igneous rocks form from the cooling of magma, either below ground (intrusive) or on the surface (extrusive). Sedimentary rocks form through the weathering of existing rocks, erosion and deposition of sediments, and compaction and cementation over time. Metamorphic rocks form from the alteration of existing rocks deep underground under high pressures and temperatures.
The document describes the three main types of rocks - igneous, sedimentary, and metamorphic. It explains that igneous rocks form from the cooling of magma, sedimentary rocks form from the compaction of sediments, and metamorphic rocks form from the alteration of existing rocks due to heat and pressure. The rock cycle is also discussed, which illustrates how rocks continuously form, change, and erode over time. Various sub-types and characteristics of each rock type are provided as examples.
The document outlines specific learning outcomes for a lesson on rock types. At the end of the lesson, students will be able to: identify and describe the three basic rock types; describe how each rock type forms and define their environments of formation; describe how rocks are transformed through the rock cycle; and identify and describe different geologic processes in the rock cycle.
The document outlines specific learning outcomes for a lesson on rock types. At the end of the lesson, students will be able to: identify and describe the three basic rock types; describe how each rock type forms and define their environments of formation; describe how rocks are transformed through the rock cycle; and identify and describe different geologic processes in the rock cycle.
Immersive Learning That Works: Research Grounding and Paths ForwardLeonel Morgado
We will metaverse into the essence of immersive learning, into its three dimensions and conceptual models. This approach encompasses elements from teaching methodologies to social involvement, through organizational concerns and technologies. Challenging the perception of learning as knowledge transfer, we introduce a 'Uses, Practices & Strategies' model operationalized by the 'Immersive Learning Brain' and ‘Immersion Cube’ frameworks. This approach offers a comprehensive guide through the intricacies of immersive educational experiences and spotlighting research frontiers, along the immersion dimensions of system, narrative, and agency. Our discourse extends to stakeholders beyond the academic sphere, addressing the interests of technologists, instructional designers, and policymakers. We span various contexts, from formal education to organizational transformation to the new horizon of an AI-pervasive society. This keynote aims to unite the iLRN community in a collaborative journey towards a future where immersive learning research and practice coalesce, paving the way for innovative educational research and practice landscapes.
Unlocking the mysteries of reproduction: Exploring fecundity and gonadosomati...AbdullaAlAsif1
The pygmy halfbeak Dermogenys colletei, is known for its viviparous nature, this presents an intriguing case of relatively low fecundity, raising questions about potential compensatory reproductive strategies employed by this species. Our study delves into the examination of fecundity and the Gonadosomatic Index (GSI) in the Pygmy Halfbeak, D. colletei (Meisner, 2001), an intriguing viviparous fish indigenous to Sarawak, Borneo. We hypothesize that the Pygmy halfbeak, D. colletei, may exhibit unique reproductive adaptations to offset its low fecundity, thus enhancing its survival and fitness. To address this, we conducted a comprehensive study utilizing 28 mature female specimens of D. colletei, carefully measuring fecundity and GSI to shed light on the reproductive adaptations of this species. Our findings reveal that D. colletei indeed exhibits low fecundity, with a mean of 16.76 ± 2.01, and a mean GSI of 12.83 ± 1.27, providing crucial insights into the reproductive mechanisms at play in this species. These results underscore the existence of unique reproductive strategies in D. colletei, enabling its adaptation and persistence in Borneo's diverse aquatic ecosystems, and call for further ecological research to elucidate these mechanisms. This study lends to a better understanding of viviparous fish in Borneo and contributes to the broader field of aquatic ecology, enhancing our knowledge of species adaptations to unique ecological challenges.
ESR spectroscopy in liquid food and beverages.pptxPRIYANKA PATEL
With increasing population, people need to rely on packaged food stuffs. Packaging of food materials requires the preservation of food. There are various methods for the treatment of food to preserve them and irradiation treatment of food is one of them. It is the most common and the most harmless method for the food preservation as it does not alter the necessary micronutrients of food materials. Although irradiated food doesn’t cause any harm to the human health but still the quality assessment of food is required to provide consumers with necessary information about the food. ESR spectroscopy is the most sophisticated way to investigate the quality of the food and the free radicals induced during the processing of the food. ESR spin trapping technique is useful for the detection of highly unstable radicals in the food. The antioxidant capability of liquid food and beverages in mainly performed by spin trapping technique.
Current Ms word generated power point presentation covers major details about the micronuclei test. It's significance and assays to conduct it. It is used to detect the micronuclei formation inside the cells of nearly every multicellular organism. It's formation takes place during chromosomal sepration at metaphase.
Or: Beyond linear.
Abstract: Equivariant neural networks are neural networks that incorporate symmetries. The nonlinear activation functions in these networks result in interesting nonlinear equivariant maps between simple representations, and motivate the key player of this talk: piecewise linear representation theory.
Disclaimer: No one is perfect, so please mind that there might be mistakes and typos.
dtubbenhauer@gmail.com
Corrected slides: dtubbenhauer.com/talks.html
ESPP presentation to EU Waste Water Network, 4th June 2024 “EU policies driving nutrient removal and recycling
and the revised UWWTD (Urban Waste Water Treatment Directive)”
EWOCS-I: The catalog of X-ray sources in Westerlund 1 from the Extended Weste...Sérgio Sacani
Context. With a mass exceeding several 104 M⊙ and a rich and dense population of massive stars, supermassive young star clusters
represent the most massive star-forming environment that is dominated by the feedback from massive stars and gravitational interactions
among stars.
Aims. In this paper we present the Extended Westerlund 1 and 2 Open Clusters Survey (EWOCS) project, which aims to investigate
the influence of the starburst environment on the formation of stars and planets, and on the evolution of both low and high mass stars.
The primary targets of this project are Westerlund 1 and 2, the closest supermassive star clusters to the Sun.
Methods. The project is based primarily on recent observations conducted with the Chandra and JWST observatories. Specifically,
the Chandra survey of Westerlund 1 consists of 36 new ACIS-I observations, nearly co-pointed, for a total exposure time of 1 Msec.
Additionally, we included 8 archival Chandra/ACIS-S observations. This paper presents the resulting catalog of X-ray sources within
and around Westerlund 1. Sources were detected by combining various existing methods, and photon extraction and source validation
were carried out using the ACIS-Extract software.
Results. The EWOCS X-ray catalog comprises 5963 validated sources out of the 9420 initially provided to ACIS-Extract, reaching a
photon flux threshold of approximately 2 × 10−8 photons cm−2
s
−1
. The X-ray sources exhibit a highly concentrated spatial distribution,
with 1075 sources located within the central 1 arcmin. We have successfully detected X-ray emissions from 126 out of the 166 known
massive stars of the cluster, and we have collected over 71 000 photons from the magnetar CXO J164710.20-455217.
The ability to recreate computational results with minimal effort and actionable metrics provides a solid foundation for scientific research and software development. When people can replicate an analysis at the touch of a button using open-source software, open data, and methods to assess and compare proposals, it significantly eases verification of results, engagement with a diverse range of contributors, and progress. However, we have yet to fully achieve this; there are still many sociotechnical frictions.
Inspired by David Donoho's vision, this talk aims to revisit the three crucial pillars of frictionless reproducibility (data sharing, code sharing, and competitive challenges) with the perspective of deep software variability.
Our observation is that multiple layers — hardware, operating systems, third-party libraries, software versions, input data, compile-time options, and parameters — are subject to variability that exacerbates frictions but is also essential for achieving robust, generalizable results and fostering innovation. I will first review the literature, providing evidence of how the complex variability interactions across these layers affect qualitative and quantitative software properties, thereby complicating the reproduction and replication of scientific studies in various fields.
I will then present some software engineering and AI techniques that can support the strategic exploration of variability spaces. These include the use of abstractions and models (e.g., feature models), sampling strategies (e.g., uniform, random), cost-effective measurements (e.g., incremental build of software configurations), and dimensionality reduction methods (e.g., transfer learning, feature selection, software debloating).
I will finally argue that deep variability is both the problem and solution of frictionless reproducibility, calling the software science community to develop new methods and tools to manage variability and foster reproducibility in software systems.
Exposé invité Journées Nationales du GDR GPL 2024
2. • Avoid making unnecessary noise.
• If you have questions, raise your
hand.
• No cell phones.
• Be active and attentive to our
discussion.
• Violating the rules above 3 times,
all of you will have a punishment.
CLASSROOM RULES
3. • Differentiate rocks according to
their type.
• Classify rocks into the three main
types: igneous, metamorphic, and
sedimentary, based on their
characteristics and formation
processes.
LEARNING OBJECTIVES
4. • Aggregate of various
types of minerals or
individual grains of the
same kind of mineral.
• Most consist of several
minerals
What is ROCK?
5. • How many minerals
can you see in this
picture?
What is ROCK?
Granite
7. Rocks are formed through LITHIFICATION
PROCESS OF ROCK FORMATION
There are 3 ways for lithification to
occur
• COMPACTION
• CEMENTATION
• RECRYSTALLIZATION
8. COMPACTION
PROCESS OF ROCK FORMATION
The consolidation of
the sediments due to
the intense pressing of
weight making the
them lose the porosity.
9. CEMENTATION
PROCESS OF ROCK FORMATION
Dissolved minerals crystallize
and glue sediments together.
Happen when ions of ground
water precipitates.
11. RECRYSTALLIZATION
PROCESS OF ROCK FORMATION
Unstable minerals recrystallize
into stable minerals that
causes grains to bind together
12. THREE MAJOR TYPES OF ROCKS
TYPES OF ROCKS
• Sedimentary Rocks
• Metamorphic Rocks
• Igneous Rocks
13. IGNEOUS ROCKS
TYPES OF ROCKS
• Molten rock material
that cools and solidify.
• Can be classified as
Extrusive and Intrusive.
14. IGNEOUS ROCKS
TYPES OF ROCKS
• Extrusive igneous rocks
• A volcanic material (lava)
that cools down in the
surface.
• Characterized by fine
grained crystals due to fast
cooling.
15. IGNEOUS ROCKS
TYPES OF ROCKS
• Intrusive igneous rocks
• Also known as plutonic
rock. A volcanic material
that cools and solidifies
underneath or under the
surface.
16. IGNEOUS ROCKS
TYPES OF ROCKS
• Intrusive igneous
rocks
• Characterize by
coarse grained
crystall due to
slow process of
cooling.
17. COMPOSITION
CLASSIFICATION OF IGNEOUS ROCKS
• FELSIC
• the light-colored (felsic)
minerals feldspar and silica in
the form of quartz. These
have more silica as a
proportion of their overall
chemical formula.
18. COMPOSITION
CLASSIFICATION OF IGNEOUS ROCKS
• INTERMEDIATE
• composition between felsic
and mafic. Contains roughly
equal amounts of light and
dark minerals.
19. COMPOSITION
CLASSIFICATION OF IGNEOUS ROCKS
• MAFIC
• It is mostly made of dark
minerals like pyroxene and
olivine, which are rich in iron
and magnesium and relatively
poor in silica.
20. COMPOSITION
CLASSIFICATION OF IGNEOUS ROCKS
• ULTRAMAFIC
• the extremely mafic rocks
composed of mostly olivine
and some pyroxene which
have even more magnesium
and iron and even less silica.
21. • ULTRAMAFIC (Coarse
grained)
• APHANITIC (Fine grained)
• PORPHYRITIC (Large
crystalls in a large matrix)
• VESICULAR (Bubbly or
frothy)
TEXTURE
CLASSIFICATION OF IGNEOUS ROCKS
23. SEDIMENTARY ROCKS
TYPES OF ROCKS
• Formed through
accumulation of sediments,
pre-existing rocks or part of
the living organisms
24. SEDIMENTARY ROCKS
CLASSIFICATION OF SEDIMENTARY ROCKS
• Formed through
accumulation of clast such
as the little broken parts of
shells and rocks.
• CLASTIC
25. SEDIMENTARY ROCKS
• Formed via the evaporation
of water and the
precipitation of ions over
time.
• CHEMICAL
CLASSIFICATION OF SEDIMENTARY ROCKS
26. SEDIMENTARY ROCKS
• Formed via accumulation of
the materials from the living
organisms .
• ORGANIC
CLASSIFICATION OF SEDIMENTARY ROCKS
27. METAMORPHIC ROCKS
TYPES OF ROCKS
• Formed from the pre-existing rocks
(igneous or sedimentary).
Metamorphic rocks form when
rocks are subjected to high heat,
high pressure, hot mineral-rich
fluids or, more commonly, some
combination of these factors.
28. METAMORPHIC ROCKS
TYPES OF ROCKS
• METAMORPHISM
it is the process of putting the
rock under high heat and
pressure without melting that
causes the geologic texture to
change.
30. TWO TYPES OF METAMORPHISM
• REGIONAL METAMORPHISM
• These rocks were typically
exposed to tectonic forces and
associated high pressures and
temperatures. Usually deformed
and foliated
31. TWO TYPES OF METAMORPHISM
• CONTACT METAMORPHISM
• Also called thermal
metamorphism by which the
country rock that surrounds a hot
magma intrusion is
metamorphosed by the high heat
flow coming from the intrusion.
32. Using Venn Diagram, compare and
contrast the three types of rocks.
ACTIVITY (1/2 CROSSWISE)
33. Search for examples (at least 5 for
each type) of the rocks.
STUDY ABOUT ROCK CYCLE FOR
RECITATION
Assignment (short B-paper)